Measure and investigate changes in the mass of ice sheets and glaciers,

Estimate and study sea ice thickness,

Measure the height of vegetation in forests and other ecosystems worldwide.

Ice

Earth’s frozen regions – the cryosphere – are changing rapidly in our warming climate. And what happens in the cryosphere does not stay in the cryosphere. Our climate depends on the poles: Disappearing sea ice can interfere with the large-scale ocean circulation patterns that buffer climate extremes. Melting glaciers and ice sheets raise sea level.

Far-Reaching Impacts

Far-Reaching Impacts

What happens in the cryosphere doesn't stay in the cryosphere - melting ice changes the global environment.

ICESat-2’s frequent, precise measurements of elevation will allow scientists to see where ice is flowing, melting or growing, and to investigate the global impacts of these changes.

Far-Reaching Impacts

What happens in the cryosphere doesn't stay in the cryosphere - melting ice changes the global environment.

ICESat-2’s frequent, precise measurements of elevation will allow scientists to see where ice is flowing, melting or growing, and to investigate the global impacts of these changes.

Ice science is a multifaceted field of study, and the ICESat-2 mission is designed to investigate the different forms of frozen water in its varied locations. Ice on land is different from ice floating on water -- land ice builds up from centuries' worth of snowfall; sea ice forms when the salty polar ocean freezes. Earth's frozen poles are different environments -- the North Pole lies within an ice-covered ocean, surrounded by land including Greenland and its ice sheet. The South Pole lies on ice-covered land, surrounded by oceans.

Earth's polar regions - The South Pole on the left and the North Pole to the right. (NASA)

ICESat-2's sole instrument, ATLAS, collects elevation data using six laser beams - which gives the new mission much denser coverage of Earth's surface.

The original ICESat had a single laser beam, collecting data in a grid shown to the left. With ICESat-2's six laser beams, the satellite will be able to take measurements in a much denser grid, as seen on the right. (NASA)

Beyond the Poles

ICESat-2 will also survey heights of the world’s forests, lakes, urban areas, cloud cover and more, adding a third dimension to flat images of Earth from space.

Other Earth-observing satellites, such as Landsat and MODIS, allow researchers to study the location and extent of forests; ICESat-2 will allow them to add the height. Because ATLAS is sensitive enough to detect individual photons, and has such a rapid firing rate, the instrument will be able to detect both the forest floor and the tops of canopies in all but the densest woods and jungles.

ICESat-2 will measure the heights of tree canopies, as well as the forest floor. (NASA)

With the new dimension, scientists can calculate the amount of vegetation – the trunks, branches, leaves, shrubs and more – that make up an area’s biomass. Studying the gain or loss of biomass can inform calculations of the carbon that forests either take in or release into the atmosphere.

The ICESat-2 mission will create a dense grid of measurements across the world, gathering information of the heights of cities, waterways, reservoirs, wetlands, agricultural fields, tundra… the satellite is always on, when it’s operational it will collect a tetrabyte of data every day.

A camera flown with one of NASA's airborne lidar, called G-LiHT, captured this view of an Alaskan forest. (NASA)

Flying over the frozen boreal plains of Canada, for example, it could detect melting of the permafrost as the thawing ground settles. Over the coastal oceans, it could detect changes in tides (CHK). With before and after measurements, it could measure ground movements following a major earthquake or volcanic eruption, or the effects of landslides and avalanches.

While ICESat-2’s laser beams can stream through some wispy clouds, other clouds will block the beam, reflecting light back to the satellite. Cloudy days aren’t necessarily bad news, however – atmospheric scientists will be able to gather information on the cloud heights, composition, density and more to advance the field of cloud physics. With the satellite's ability to detect elevation change on such a fine scale, scientists are expecting the data will lead to unexpected new discoveries.

On the Shoulders of ICESat

From 2003 to 2009, the ICESat mission provided multi-year elevation data needed to determine ice sheet mass balance as well as cloud property information, especially for stratospheric clouds common over polar areas. It also provided topography and vegetation data around the globe, in addition to the polar-specific coverage over the Greenland and Antarctic ice sheets.

Following ICESat, NASA began an airborne campaign called Operation IceBridge. The mission of IceBridge is to collect data on changing polar land and sea ice and maintain continuity of measurements between the first ICESat and ICESat-2 missions. IceBridge, which began in in 2009, is currently funded until 2019. The planned two-year overlap with ICESat-2 will help scientists validate the satellite’s measurements.

Illustration of the first ICESat. (NASA)

The extensive data IceBridge has gathered over the Greenland ice sheet during its six years of operations have provided an improved picture of the surface, the bed and the internal structures of Greenland’s ice sheet and allowed scientists to create more accurate models of glacier contribution to sea level rise. As for sea ice, IceBridge’s measurements of the thickness of sea ice and its snow cover have assisted in improving forecasts for summertime melt, enhanced the understanding of variations in ice thickness distribution from year to year, and up-dated the climatology of the snow depth over sea ice. IceBridge also flies yearly campaigns to measure the Antarctic ice sheet and surrounding sea ice.

Operation IceBridge has used several different planes to collect measurements, including this one during an Alaska campaign to study mountain glaciers. (Courtesy Chris Larsen, University of Alaska-Fairbanks)